Baker; Dock; J. Brauer; T. Lake Est. Avery; M. Sears; Green St. Kaynor; Kane Est. Kane Est. Lamkin; Washington St. Chase; M. Perry; H. Dickinson; Jos. Caywood; Adam Boburn; Division St. Brownell Est. Blake; Maple St. Electric ; G. Austin; I. Brown; Bap. Church; Parsonage; E. Wills; J. Yard; Town Hall; Pearl St. Lortie; C. Blake; J. White; Levy Devall; M. Lortie; Frank Barnes; J. Dow; W. Pierce; H. Coville; W. McClary; Fullerton; Stone; J. Allen; H. Carson; W. Harrison; A. Stafford; J. Wood; E.
Reed; F. Lortie; M. Lortie; W. Kirby; E. Harback; Levy Devall; Ada L. Draper; H. Gray; H. Moore; H. Blair; A. Boyce; G. Bowman; Main St. Bement; R. Rice; Hunt; Ford; M. Lawrence; S. Dunn; Geo. Burroughs; John Blake; Jas. Blake; N. Towne; A. Steward; J. Ross; Grove ST. Russell; E.
Hobb; J. Allen; J. Imus; C. Tillotson; F. Howell; O. Evans; Cong. Church; Church St. Mack; H. Walker; E. Curtis; T. Clapp; J. Sellman; J. Freer; C. Clapp; Res. Blake; School St. Streater; Battle Creek St. Ford; E. Dawley; W. Ford; O. McClary; F. Hawver; Wm. Blake; A. Zinn; H. Olin; Walter Cogin; M. Church Parsonage; M. Brown; L. Rogers; Cong.
Parsonage; R. Schroder; P. Muhlenburg Office; Mill; A. Schroder; W. Blake; John Schroder; Charleston Twp. Crittenden; W. Elsey; Jesse Milks; Geo. Struble; John Schroder; Josephine E. Ransom; Pierce St. Sherman; Elevator; Creamery; Geo. Smith; W. Eldred; Straus Bros. Gould; Hancock St. Sinclair; Note:. Kenyon; H. Miller; Kenyon St. Church Prop. Walker; J. Longer; E. Kenyon; Prairie St. Frakes; McKain St. Briggs Est. Briggs Estate; H. Barnes; Mrs. Mich Ave. Vine St. Best; O. Briggs; Geo. Wandell; Robert Baker; S. Wing; D. Porter; Mrs. Loveseth; R. Know; McAllister; Elect. Hudson Produce; Salting Sta.
Spade; W. Gorwin; Mrs. Draper; Lee Paper Co. Wing; E. Kimbee; J. Hawkins; Mrs. Martin; Florence Clapp; J. Clapp; H. Daniels; W. Notley; Francis Notley; M. Hill; T. Raynor Est. Coller; E. Page; Prairie St. Kimble; D. Smith; E, Himebaugh; Mrs. Hill; Fred Dentler; T. Kimble; C. Pursel; P. Franklin; J. Weinberg; G. White; F. Lyons; Geo. Bond; Mrs. Bohnen; E. Erwine; E. Goldsmith; Mrs. Osborn; P. Dent; J. Hazzard; Chas. Vroman; C. Morse; F.
Shick; C. McKain; Mrs. Gleason; E. Clark; R. Kimble; E. Kenyon; J. Allen; T. Etts; W. Smith; J. Sorenson Jr. McEllisworth; J. Godsonalk; Durkee House; Vicksburg G. Mimble; J. Kimble; W. Notley; A. Ryan; Mrs. Barker; Mrs. Peterman; V. Lyon; Mrs. Knapp; Florence Smith; H. Nash; Mrs. Turner; C. Spataing; S. Wing; Vicksburg Lumber; Schoolcraft Twp. McElvain; A. Brockway; W. Brockway; A. Brockway; J. McElvain; Maple St. Brockway; Frank Clark; W.
Notley; Mrs. Beebe; P. Nuff; W. Beebe; Mrs. Mandigo; Chas. Clark; School; Park St. Cady; Mrs. Swan; G. Pearman; Mrs. Brown; South St. Woldendorp; Cemetery; Mrs. Cooley; Mrs. Harriger; H. Stofflet; T. McLeary; T. McLeary; Mrs. Scott; Mrs. Harriger; Wm. Camp; D. Dell; West Raymond St.
Darling; John Hodgson; W. Smith; G. Clark; Mrs. Harriger; City Gravel Pit; M. Hamilton; J. Clapp; G. Reed; Bishop Creamery; Geo. Reed; C. Goostry; Gill; J. Reed; I. Burk; Highway; Wayland St. Dell; Lee Paper Co. Daniels; F. Rapp; A. Findley; T. Hayes; Dentler Bagger Works; L. Rapp; Freight House; Rose St. Kern; Elevator; Vine St. Collins; L. Rapp; L. Lawrence; Mrs. Munn; Vicksburg; M. Wing; F. Fenstermacher; Hobart St. Wing; M. Fenstermacher; E. Davidson; Center St. Scott; Davis St. Symmonds; E Powers; W. White; Mill Pond; G.
Harrison; Grand Trunk R. Church; Walnut St. McKain; W. Hoag; T. Cloney; E. Peck; H. Gilson; A. Cobern; H. Wilson; H. Schuyler; H. Fisher; A. Furbush; V. Ramsdell; Dr. Braden; Dr. Braden; C. Dewey; P. Foster; Original Town; Scott St. Moor; Mary Brockway; Wm. Robinson; H. Van Vranken; Meth. Church; Office; Dr. Gifford; Harry Williams; R. Norton; Blks. Shop; J. Snyder; Elwood Peck; Groc.
Campbell; Hall; A. Griffith; Tel. Hackley; R. Garrison; R. Norton; T. Bowman; School; F. Wilson; Gen. Church; Town Hall; Cong. Church; Cemetery; J. Edwards; J. Dekema; Church; School; I. Wood; Town Hall; Main St. Southwell; Depot; Depot St. Thompson; Centre St. Burnham; W. Piper; A. Allen; R. Kenfield; J. Kent; E. Abbott; Michigan Central R. Goddes; Henry Wait; Monroe St. Burnham; Village; J. Scudder; McKay Est. Faude; Elm St. Scudder; Washington St. Fields; H. Parsonage; Jackson St.
Roster; Res. Pool; Church; Canal; Fulton St. Houvener; Res. Woods; Gen. Mdse; Park; Res. Marvin; H. Woer; Clinton St. Hudson; C. Manchester; Fayette St. Marvin; Lbr. Yard; Depot; Frewht House; Cass. Marvin; Warehouse; Carrol St. Bailey; Lincoln St. Bishop; Short St. Gould; J. Hudson Packg. House; J. Miller; Charleston Twp. Scudder; Deckland; Thos. Hobden; W. Buell; C. Atwater; Tom Page; A.
Owen; H. Kent; M. Gibbs; H. Ralston; State St. McGuin; J. Van Antwerpen; C. Richard; S. Green; H. Gales; M. Hudson; R. Crossfield; M. Church; State St. Rickard; F. Hanson; M. Foote; A. Troy; B. Crandall; Church St. Shop; W. Boiles; Mary Hardman; E. Thompson; E. Haynes; Geo. Bushnell; H. Logan; Mrs. Wollsay; Frank Warnen; H. Miller; Feed Mill; J. Holden; Post Office; N. Kinney; N. Drummond; A. Burgard; K. Clapp; E. Sargent; Bakery; J. Southerland; N. Multispectral digital classifications of land cover features indicative of floodplain areas were used by interpreters to locate various floodprone area boundaries.
Results indicate that remote sensing techniques can delineate floodprone areas more easily in agricultural and limited development areas as opposed to areas covered by a heavy forest canopy. At this time it appears that the remote sensing data would be best used as a form of preliminary planning information or as an internal check on previous or ongoing floodplain studies. In addition, the remote sensing techniques can assist in effectively monitoring floodplain activities after a community enters into the National Flood Insurance Program.
Aerial radiometric and magnetic reconnaissance survey of a portion of Texas: Beaumont and Palestine quadrangles, final report. Volume 1 and Volume 2A, Beaumont quadrangle. Instrumentation and methods described were used for a Department of Energy DOE sponsored, high-sensitivity, aerial gamma-ray spectrometer and magnetometer survey of a portion of Beaumont and all of Palestine Texas , NTMS, ,scale quadrangles.
The objective of the work was to define areas showing surface indications of a generally higher uranium content where detailed exploration for uranium would most likely be successful. A DC-3 aircraft equipped with a high-sensitivity gamma-ray spectrometer and ancillary geophysical and electronic equipment ws employed for each quadrangle. Results of the interpretation in the form of a preferred-anomaly map, along with significance-factor profile maps, stacked profiles, histograms, and descriptions of the geology and known uranium occurrences are presented in Volume 2 of this final report.
Volume 1 and Volume 2B, Palestine quadrangle. A DC-3 aircraft equipped with a high-sensitivity gamma-ray spectrometer and ancillary geophysical and electronic equipment was employed for each quadrangle. Volume 2-F.
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Lewistown Quadrangle. Results of a high-sensitivity, aerial, gamma-ray spectrometer and magnetometer survey of the Lewistown Quadrangle, Montana, are presented. Statistical and geological analysis of the radiometric data revealed 58 uranium anomalies worthy of field-checking as possible prospects. One anomaly may be associated with the Cambrian Flathead Quartzite that may contain deposits similar to the Blind River and Rand uranium deposits.
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Three anomalies may be indicative of sandstone-type deposits in Jurassic rocks, particularly the Morrison Formation, which hosts uranium mineralization elsewhere. There are 45 anomalies related to the Cretaceous rocks. Lignite in the Hell Creek and Judith River formations and Eagle Sandstone may have caused the formation of 22 epigenetic uranium deposits. Many anomalies occur in the Bearpaw Shale and Claggett Formation. However, only five are considered significant of the remainder are expected to be caused by large amounts of radioactive bentonite or bentonitic shale.
Two other Cretaceous units that may host sandstone-type deposits are the Colorado Shale and Kootenai Formation that register 16 and two anomalies respectively. Only one anomaly pertains to Tertiary rocks, and it may be indicative of vein-type deposits in the intrusives of the Judith Mountains.
These rocks may also act as source rocks for deposits surrounding the Judith Mountains.
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Eight anomalies related only to Quaternary units may be demonstrative of uranium-rich source rocks that could host uranium mineralization. Several anomalies are located close to oil fields and may have been cause by radium-rich oil-field brines. A diver reconnaissance of the intertidal and subtidal zones of Back Island was performed to catalog potentially vulnerable shellfish, other invertebrates, and marine plant resources occurring at three proposed alternate pier sites on the west side of Back Island.
Additionally, a limited survey of terrestrial vegetation was conducted in the vicinity of one of the proposed alternate pier sites to describe the littoral community and to list the dominant plant species found there. Box Walrus foraging marks on the seafloor in Bristol Bay, Alaska: A reconnaissance survey. Bornhold, Brian D. A reconnaissance sidescan sonar survey in Bristol Bay, Alaska revealed extensive areas of seafloor with features related to walrus foraging. They are similar to those seen in areas such as the outer Bering Sea and Chukchi Sea.
The distribution of foraging marks was consistent in a general way with walrus locations from satellite telemetry studies. Volume II. New Mexico-Roswell NI quadrangle. The results of a high-sensitivity, aerial gamma-ray spectrometer and magnetometer survey of the Roswell two degree quadrangle, New Mexico are presented. Instrumentation and methods are described in Volume I of this final report. The work was done by Carson Helicopters, Inc. Analysis of this radiometric data yielded statistically significant eU anomalies. Of this number, seventy-four were considered to be sufficient strength to warrant further investigation.
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The results of a high-sensitivity, aerial gamma-ray spectrometer and magnetometer survey of the Fort Sumner, two degree quadrangle, New Mexico, are presented. The work was done by Carson Helicopters Inc. A total of statistically significant eU anomalies were identified in this quadrangle. Of this number 31 were considered to be of sufficient intensity to warrant field investigations.
Arizona-Holbrook NI Quadrangle. The results of a high-sensitivity, aerial gamma-ray spectrometer and magnetometer survey of the Holbrook two degree quadrangle, Arizona are presented. Of this number, forty-four were considered to be of sufficient strength to warrant further investigation. The results of a high-sensitivity, aerial gamma-ray spectrometer and magnetometer survey of the El Paso, two degree quadrangle, New Mexico, are presented. A total of 72 statistically significant eU anomalies were identified in this quadrangle. Only three of the 20 can, with certainty be identified with bedrock; one with a Quaternary flow, one with Cambrian sandstone and one with a Precambrian granite.
Reconnaissance survey of the Duolun ring structure in Inner Mongolia: Not an impact structure. The Duolun basin, which is located in Inner Mongolia, China, has been proposed to be an impact structure with an apparent rim diameter of about 70, or even km.
The designation as an impact structure was based on its nearly circular topography, consisting of an annular moat that surrounds an inner hummocky region, and the widespread occurrences of various igneous rocks, polymict breccias, and deformed crustal rocks. Critical shock metamorphic evidence is not available to support the impact hypothesis. We conducted two independent reconnaissance field surveys to this area and studied the lithology both within and outside of the ring structure.
We collected samples from all lithologies that might contain evidence of shock metamorphism as suggested by their locations, especially those sharing similar appearances with impact breccias, suevites, impact melt rocks, and shatter cones.
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Field investigation, together with thin-section examination, discovered that the suspected impact melt rocks are actually Early Cretaceous and Late Jurassic lava flows and pyroclastic deposits of rhyolitic to trachytic compositions, and the interpreted impact glass is typical volcanic glass. Petrographic analyses of all the samples reveal no indications for shock metamorphic overprint. All these lines of evidence suggest that the Duolun basin was not formed through impact cratering. The structural deformation and spatial distribution pattern of the igneous rocks suggest that the Duolun basin is most likely a Jurassic-Cretaceous complex rhyolite caldera system that has been partly filled with sediments forming an annular basin, followed by resurgent doming of the central area.
Combined with oceanographic and sea ice components of Vertical lines show median errors for forecast and climatology, respectively Figure 7 Correlation coefficient. Geologic reconnaissance and geochemical sampling survey of molybdenum mineralization near Schiestler Peak, Temple Peak Quadrangle, Sublette County, Wyoming. A brief geologic reconnaissance and geochemical survey of molybdenum mineralization near Schiestler Peak, Sublette County, Wyo.
Samples of stream sediments, panned concentrates from stream sediments, soils, rocks, and water were collected in the geochemical survey.
Analytical results show that in reconnaissance , panned concentrates are the best of the sample types used in this study to detect molybdenum mineralization. More detailed analysis of the distribution of the molybdenum is best achieved through the collection of rock samples. Hydrothermal alteration is generally not conspicuous in the study area; however, rock samples that contain molybdenite are usually slightly enriched in silver, copper, lead, and in several instances, gold. Conversely, there appear to be negative associations between molybdenum and zinc and between molybdenum and several of the rare-earth elements.
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Mo concentrations in the rock samples with no visible molybdenite range from undetectable at a sensitivity of 5 parts per million ppm to ppm. Mo content in rock samples containing visible molybdenite ranges from 10 ppm to greater than 2, ppm. Stream-sediment values range from undetected to 15 ppm; panned concentrates from undetected to 15 ppm; soils from undetected to 20 ppm. Analyses of the water samples indicate Mo concentrations from 0.
As currently understood, this deposit is not extensive or continuous, but drilling to provide information on the vertical extent of mineralization may alter this opinion. The projects i dentified These changes in turn will affect the evolution of the SIZ. An appropriate representation of this feedback loop in models is critical if we In the present survey , geochemical anomalies locate all the sites of mineralization known from previous work. The survey is therefore technically a success.
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However, a large number of these anomalies probably result from contamination of the wadi systems by metal dispersed from ancient mine workings, and this particular survey , overall, may be of limited value as a guide to the discovery of hitherto unknown mineralization. Nevertheless, the survey outlines two areas that may mark extensions to known mineralization, and a number of other areas in which no mineralization is known.
Based on a consideration of the character of the bedrock geology, the value of each reported analytical result in relation to the respective element thresholds, and the number of anomalous samples that cluster in any given area, four areas are recommended for high-priority follow-up sampling.
Audio-magnetotelluric methods in reconnaissance geothermal exploration.